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Typically, this rate of increase slows after about 10,000 years, plant nutrients begin to leach away, and a significant decline in humus content is observed for soils whose age approaches one million years.
No significant effect of salt content is observed.
A linear decrease of the Er content is observed.
The nitrogen content is observed to decrease with increasing substrate temperature.
The common trend of glass transition changing with amino-MMT content is observed.
By examining the X-ray photoelectron spectroscopy (XPS) spectrum, different non-lattice oxygen content is observed.
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However, no correlation to soluble phenolic content was observed.
A net increase of 17.57 % in chromium content was observed.
In Figure 6A, no abnormal DNA content was observed.
A corresponding increase in the ash content was observed.
A decrease in the soft α-Fe phase content was observed after infiltration.
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